Geoscience ›› 2022, Vol. 36 ›› Issue (03): 836-847.DOI: 10.19657/j.geoscience.1000-8527.2021.147
• Petrology • Previous Articles Next Articles
LÜ Yunhe(), DONG Guochen(
), ZHAO Liwei, SU Lin, YIN Guodong, TANG Jiahui
Received:
2021-07-08
Revised:
2021-12-18
Online:
2022-06-10
Published:
2022-07-19
CLC Number:
LÜ Yunhe, DONG Guochen, ZHAO Liwei, SU Lin, YIN Guodong, TANG Jiahui. Formation Age and Magma Source of the Shazhangtu Diorite Porphyry, Inner Mongolia: Constraints of Petrogeochemistry, Zircon U-Pb Geochronology and Hf Isotopes[J]. Geoscience, 2022, 36(03): 836-847.
分析点 | 元素含量/10-6 | Th/U | 同位素比值 | 年龄/Ma | |||||||
---|---|---|---|---|---|---|---|---|---|---|---|
Th | U | Pb | 207Pb/206Pb±1σ | 207Pb/235U±1σ | 206Pb/238U±1σ | 207Pb/235U ±1σ | 206Pb/238U ±1σ | ||||
IIML84-01 | 129.2 | 273.9 | 15.2 | 0.5 | 0.051 77±0.000 98 | 0.350 94±0.007 07 | 0.049 11±0.000 44 | 305.4±5.3 | 309.1±2.7 | ||
IIML84-02 | 144.6 | 315.6 | 17.5 | 0.5 | 0.051 50±0.000 95 | 0.351 99±0.006 33 | 0.049 61±0.000 39 | 306.2±4.8 | 312.1±2.4 | ||
IIML84-03 | 89.2 | 235.4 | 13.0 | 0.4 | 0.052 32±0.001 06 | 0.360 82±0.007 16 | 0.050 03±0.000 40 | 312.8±5.3 | 314.7±2.5 | ||
IIML84-04 | 176.7 | 435.4 | 24.1 | 0.4 | 0.051 10±0.000 83 | 0.356 33±0.006 15 | 0.050 52±0.000 50 | 309.5±4.6 | 317.7± 3.1 | ||
IIML84-05 | 61.2 | 159.6 | 8.8 | 0.4 | 0.051 56±0.001 13 | 0.357 30±0.007 72 | 0.050 33±0.000 52 | 310.2±5.8 | 316.5±3.2 | ||
IIML84-06 | 117.0 | 258.2 | 14.1 | 0.5 | 0.053 68±0.001 16 | 0.364 53±0.008 06 | 0.049 22±0.000 50 | 315.6±6.0 | 309.7±3.1 | ||
IIML84-07 | 93.3 | 233.7 | 12.8 | 0.4 | 0.052 49±0.001 10 | 0.363 94±0.007 20 | 0.050 36±0.000 51 | 315.2±5.4 | 316.7±3.1 | ||
IIML84-08 | 167.1 | 315.5 | 17.7 | 0.5 | 0.052 90±0.000 93 | 0.361 05±0.006 33 | 0.049 38±0.000 42 | 313.0±4.7 | 310.7±2.6 | ||
IIML84-09 | 122.5 | 313.0 | 16.8 | 0.4 | 0.052 47±0.000 84 | 0.359 06±0.005 78 | 0.049 53±0.000 44 | 311.5±4.3 | 311.6±2.7 | ||
IIML84-10 | 128.0 | 258.8 | 14.4 | 0.5 | 0.051 91±0.000 95 | 0.353 38±0.006 78 | 0.049 26±0.000 46 | 307.3±5.1 | 310.0±2.8 | ||
IIML84-11 | 82.0 | 218.6 | 11.9 | 0.4 | 0.051 57±0.001 11 | 0.354 71±0.007 14 | 0.049 98±0.000 47 | 308.3±5.4 | 314.4±2.9 | ||
IIML84-12 | 129.7 | 288.8 | 15.7 | 0.4 | 0.056 18±0.001 12 | 0.381 73±0.007 61 | 0.049 27±0.000 53 | 328.3±5.6 | 310.0±3.3 | ||
IIML84-13 | 151.4 | 257.0 | 14.9 | 0.6 | 0.051 03±0.001 10 | 0.355 94±0.007 21 | 0.050 65±0.000 48 | 309.2±5.4 | 318.5±3.0 | ||
IIML84-14 | 90.5 | 236.9 | 12.9 | 0.4 | 0.053 07±0.001 07 | 0.360 40±0.007 05 | 0.049 20±0.000 46 | 312.5±5.3 | 309.6±2.8 | ||
IIML84-15 | 65.3 | 204.2 | 10.9 | 0.3 | 0.050 91±0.001 16 | 0.351 04±0.007 85 | 0.050 02±0.000 52 | 305.5±5.9 | 314.6±3.2 | ||
IIML84-16 | 202.4 | 358.3 | 20.4 | 0.6 | 0.051 58±0.000 92 | 0.351 25±0.005 83 | 0.049 42±0.000 43 | 305.7±4.4 | 311.0±2.6 | ||
IIML84-17 | 89.0 | 207.3 | 11.2 | 0.4 | 0.052 10±0.001 22 | 0.349 51±0.008 04 | 0.048 64±0.000 45 | 304.4±6.1 | 306.2±2.8 | ||
IIML84-18 | 73.0 | 164.8 | 9.2 | 0.4 | 0.050 32±0.001 26 | 0.338 51±0.008 41 | 0.048 81±0.000 51 | 296.0±6.4 | 307.2±3.2 | ||
IIML84-19 | 117.1 | 261.9 | 14.6 | 0.4 | 0.051 50±0.001 08 | 0.354 10±0.007 33 | 0.049 88±0.000 48 | 307.8±5.5 | 313.8±3.0 | ||
IIML84-20 | 94.8 | 230.6 | 12.9 | 0.4 | 0.052 30±0.001 20 | 0.362 69±0.008 44 | 0.050 26±0.000 45 | 314.2±6.3 | 316.1±2.8 |
Table 1 LA-ICP-MS zircon U-Pb data of the diorite porphyrite in Shazhangtu mining area
分析点 | 元素含量/10-6 | Th/U | 同位素比值 | 年龄/Ma | |||||||
---|---|---|---|---|---|---|---|---|---|---|---|
Th | U | Pb | 207Pb/206Pb±1σ | 207Pb/235U±1σ | 206Pb/238U±1σ | 207Pb/235U ±1σ | 206Pb/238U ±1σ | ||||
IIML84-01 | 129.2 | 273.9 | 15.2 | 0.5 | 0.051 77±0.000 98 | 0.350 94±0.007 07 | 0.049 11±0.000 44 | 305.4±5.3 | 309.1±2.7 | ||
IIML84-02 | 144.6 | 315.6 | 17.5 | 0.5 | 0.051 50±0.000 95 | 0.351 99±0.006 33 | 0.049 61±0.000 39 | 306.2±4.8 | 312.1±2.4 | ||
IIML84-03 | 89.2 | 235.4 | 13.0 | 0.4 | 0.052 32±0.001 06 | 0.360 82±0.007 16 | 0.050 03±0.000 40 | 312.8±5.3 | 314.7±2.5 | ||
IIML84-04 | 176.7 | 435.4 | 24.1 | 0.4 | 0.051 10±0.000 83 | 0.356 33±0.006 15 | 0.050 52±0.000 50 | 309.5±4.6 | 317.7± 3.1 | ||
IIML84-05 | 61.2 | 159.6 | 8.8 | 0.4 | 0.051 56±0.001 13 | 0.357 30±0.007 72 | 0.050 33±0.000 52 | 310.2±5.8 | 316.5±3.2 | ||
IIML84-06 | 117.0 | 258.2 | 14.1 | 0.5 | 0.053 68±0.001 16 | 0.364 53±0.008 06 | 0.049 22±0.000 50 | 315.6±6.0 | 309.7±3.1 | ||
IIML84-07 | 93.3 | 233.7 | 12.8 | 0.4 | 0.052 49±0.001 10 | 0.363 94±0.007 20 | 0.050 36±0.000 51 | 315.2±5.4 | 316.7±3.1 | ||
IIML84-08 | 167.1 | 315.5 | 17.7 | 0.5 | 0.052 90±0.000 93 | 0.361 05±0.006 33 | 0.049 38±0.000 42 | 313.0±4.7 | 310.7±2.6 | ||
IIML84-09 | 122.5 | 313.0 | 16.8 | 0.4 | 0.052 47±0.000 84 | 0.359 06±0.005 78 | 0.049 53±0.000 44 | 311.5±4.3 | 311.6±2.7 | ||
IIML84-10 | 128.0 | 258.8 | 14.4 | 0.5 | 0.051 91±0.000 95 | 0.353 38±0.006 78 | 0.049 26±0.000 46 | 307.3±5.1 | 310.0±2.8 | ||
IIML84-11 | 82.0 | 218.6 | 11.9 | 0.4 | 0.051 57±0.001 11 | 0.354 71±0.007 14 | 0.049 98±0.000 47 | 308.3±5.4 | 314.4±2.9 | ||
IIML84-12 | 129.7 | 288.8 | 15.7 | 0.4 | 0.056 18±0.001 12 | 0.381 73±0.007 61 | 0.049 27±0.000 53 | 328.3±5.6 | 310.0±3.3 | ||
IIML84-13 | 151.4 | 257.0 | 14.9 | 0.6 | 0.051 03±0.001 10 | 0.355 94±0.007 21 | 0.050 65±0.000 48 | 309.2±5.4 | 318.5±3.0 | ||
IIML84-14 | 90.5 | 236.9 | 12.9 | 0.4 | 0.053 07±0.001 07 | 0.360 40±0.007 05 | 0.049 20±0.000 46 | 312.5±5.3 | 309.6±2.8 | ||
IIML84-15 | 65.3 | 204.2 | 10.9 | 0.3 | 0.050 91±0.001 16 | 0.351 04±0.007 85 | 0.050 02±0.000 52 | 305.5±5.9 | 314.6±3.2 | ||
IIML84-16 | 202.4 | 358.3 | 20.4 | 0.6 | 0.051 58±0.000 92 | 0.351 25±0.005 83 | 0.049 42±0.000 43 | 305.7±4.4 | 311.0±2.6 | ||
IIML84-17 | 89.0 | 207.3 | 11.2 | 0.4 | 0.052 10±0.001 22 | 0.349 51±0.008 04 | 0.048 64±0.000 45 | 304.4±6.1 | 306.2±2.8 | ||
IIML84-18 | 73.0 | 164.8 | 9.2 | 0.4 | 0.050 32±0.001 26 | 0.338 51±0.008 41 | 0.048 81±0.000 51 | 296.0±6.4 | 307.2±3.2 | ||
IIML84-19 | 117.1 | 261.9 | 14.6 | 0.4 | 0.051 50±0.001 08 | 0.354 10±0.007 33 | 0.049 88±0.000 48 | 307.8±5.5 | 313.8±3.0 | ||
IIML84-20 | 94.8 | 230.6 | 12.9 | 0.4 | 0.052 30±0.001 20 | 0.362 69±0.008 44 | 0.050 26±0.000 45 | 314.2±6.3 | 316.1±2.8 |
样号 | SiO2 | TiO2 | Al2O3 | TFe2O3 | MnO | MgO | CaO | Na2O | K2O | P2O5 | 烧失量 | 总量 | A/CNK | A/NK | AR | σ |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
IIML42 | 60.45 | 0.87 | 16.64 | 9.04 | 0.06 | 1.92 | 2.52 | 2.29 | 3.01 | 0.29 | 2.47 | 99.56 | 1.43 | 2.37 | 1.63 | 1.55 |
IIML84 | 56.52 | 1.02 | 16.85 | 9.09 | 0.12 | 3.58 | 4.45 | 2.72 | 3.01 | 0.29 | 1.90 | 99.55 | 1.06 | 2.18 | 1.69 | 2.31 |
IIML88 | 56.19 | 1.03 | 17.31 | 9.46 | 0.13 | 3.32 | 4.68 | 2.54 | 2.43 | 0.31 | 2.57 | 99.97 | 1.13 | 2.54 | 1.58 | 1.77 |
IIML89 | 56.24 | 0.97 | 17.01 | 9.42 | 0.12 | 3.38 | 5.26 | 2.74 | 1.94 | 0.28 | 2.36 | 99.72 | 1.05 | 2.57 | 1.53 | 1.56 |
IIML90 | 56.96 | 1.01 | 16.81 | 8.37 | 0.15 | 3.54 | 5.22 | 2.85 | 2.48 | 0.26 | 1.79 | 99.44 | 1.00 | 2.28 | 1.64 | 1.94 |
Table 2 Major elements (%) analysis results of the diorite porphyrite in Shazhangtu mining area
样号 | SiO2 | TiO2 | Al2O3 | TFe2O3 | MnO | MgO | CaO | Na2O | K2O | P2O5 | 烧失量 | 总量 | A/CNK | A/NK | AR | σ |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
IIML42 | 60.45 | 0.87 | 16.64 | 9.04 | 0.06 | 1.92 | 2.52 | 2.29 | 3.01 | 0.29 | 2.47 | 99.56 | 1.43 | 2.37 | 1.63 | 1.55 |
IIML84 | 56.52 | 1.02 | 16.85 | 9.09 | 0.12 | 3.58 | 4.45 | 2.72 | 3.01 | 0.29 | 1.90 | 99.55 | 1.06 | 2.18 | 1.69 | 2.31 |
IIML88 | 56.19 | 1.03 | 17.31 | 9.46 | 0.13 | 3.32 | 4.68 | 2.54 | 2.43 | 0.31 | 2.57 | 99.97 | 1.13 | 2.54 | 1.58 | 1.77 |
IIML89 | 56.24 | 0.97 | 17.01 | 9.42 | 0.12 | 3.38 | 5.26 | 2.74 | 1.94 | 0.28 | 2.36 | 99.72 | 1.05 | 2.57 | 1.53 | 1.56 |
IIML90 | 56.96 | 1.01 | 16.81 | 8.37 | 0.15 | 3.54 | 5.22 | 2.85 | 2.48 | 0.26 | 1.79 | 99.44 | 1.00 | 2.28 | 1.64 | 1.94 |
样品编号 | La | Ce | Pr | Nd | Sm | Eu | Gd | Tb | Dy | Ho | Er | Tm |
---|---|---|---|---|---|---|---|---|---|---|---|---|
IIML42 | 28.94 | 59.11 | 6.97 | 28.29 | 6.29 | 1.24 | 5.83 | 0.92 | 5.43 | 0.97 | 2.82 | 0.45 |
IIML84 | 24.30 | 53.91 | 6.76 | 29.17 | 6.31 | 1.95 | 5.79 | 0.94 | 5.51 | 1.09 | 3.10 | 0.44 |
IIML88 | 25.16 | 51.97 | 6.60 | 28.19 | 6.22 | 1.91 | 6.04 | 0.95 | 5.38 | 1.00 | 2.73 | 0.41 |
IIML89 | 25.65 | 55.21 | 6.98 | 28.86 | 6.32 | 1.80 | 5.56 | 0.85 | 5.10 | 1.01 | 2.88 | 0.42 |
IIML90 | 26.11 | 55.20 | 6.83 | 29.39 | 6.76 | 1.87 | 6.26 | 1.01 | 5.64 | 1.04 | 2.89 | 0.43 |
样品编号 | Yb | Lu | Y | REE | LREE | HREE | LREE/ HREE | (La/Yb)N | (La/Sm)N | (Gd/Lu)N | δEu | δCe |
IIML42 | 2.98 | 0.43 | 31.50 | 150.67 | 130.85 | 19.82 | 6.60 | 6.96 | 2.97 | 1.69 | 0.63 | 1.02 |
IIML84 | 2.93 | 0.42 | 30.42 | 142.62 | 122.40 | 20.22 | 6.05 | 5.95 | 2.49 | 1.71 | 0.98 | 1.03 |
IIML88 | 2.67 | 0.39 | 29.98 | 139.62 | 120.04 | 19.58 | 6.13 | 6.75 | 2.61 | 1.93 | 0.95 | 0.99 |
IIML89 | 2.89 | 0.43 | 28.89 | 143.94 | 124.80 | 19.14 | 6.52 | 6.37 | 2.62 | 1.60 | 0.93 | 1.01 |
IIML90 | 2.91 | 0.41 | 31.12 | 146.75 | 126.16 | 20.59 | 6.13 | 6.44 | 2.49 | 1.88 | 0.88 | 1.01 |
样品编号 | Rb | Ba | Th | U | K | Ta | Nb | Sr | P | Zr | Hf | Ti |
IIML42 | 288.25 | 341.70 | 9.35 | 2.23 | 25 741.60 | 0.80 | 11.35 | 209.49 | 1 310.70 | 219.10 | 5.61 | 5 376.90 |
IIML84 | 210.93 | 310.53 | 7.09 | 2.04 | 25 588.81 | 0.84 | 10.99 | 478.30 | 1 294.78 | 282.57 | 6.39 | 6 261.00 |
IIML88 | 144.13 | 281.42 | 6.57 | 2.24 | 20 711.10 | 0.74 | 10.36 | 388.47 | 1 387.63 | 270.59 | 6.39 | 6 338.61 |
IIML89 | 92.83 | 292.51 | 7.46 | 1.97 | 16 541.58 | 0.78 | 10.9 | 459.31 | 1 253.86 | 285.18 | 6.70 | 5 971.83 |
IIML90 | 139.32 | 373.38 | 7.10 | 1.92 | 21 083.14 | 0.82 | 11.37 | 487.04 | 1 160.84 | 296.11 | 6.61 | 6 199.62 |
Table 3 Rare earth element (10-6) and trace element (10-6) data of the diorite porphyrite in Shazhangtu mining area
样品编号 | La | Ce | Pr | Nd | Sm | Eu | Gd | Tb | Dy | Ho | Er | Tm |
---|---|---|---|---|---|---|---|---|---|---|---|---|
IIML42 | 28.94 | 59.11 | 6.97 | 28.29 | 6.29 | 1.24 | 5.83 | 0.92 | 5.43 | 0.97 | 2.82 | 0.45 |
IIML84 | 24.30 | 53.91 | 6.76 | 29.17 | 6.31 | 1.95 | 5.79 | 0.94 | 5.51 | 1.09 | 3.10 | 0.44 |
IIML88 | 25.16 | 51.97 | 6.60 | 28.19 | 6.22 | 1.91 | 6.04 | 0.95 | 5.38 | 1.00 | 2.73 | 0.41 |
IIML89 | 25.65 | 55.21 | 6.98 | 28.86 | 6.32 | 1.80 | 5.56 | 0.85 | 5.10 | 1.01 | 2.88 | 0.42 |
IIML90 | 26.11 | 55.20 | 6.83 | 29.39 | 6.76 | 1.87 | 6.26 | 1.01 | 5.64 | 1.04 | 2.89 | 0.43 |
样品编号 | Yb | Lu | Y | REE | LREE | HREE | LREE/ HREE | (La/Yb)N | (La/Sm)N | (Gd/Lu)N | δEu | δCe |
IIML42 | 2.98 | 0.43 | 31.50 | 150.67 | 130.85 | 19.82 | 6.60 | 6.96 | 2.97 | 1.69 | 0.63 | 1.02 |
IIML84 | 2.93 | 0.42 | 30.42 | 142.62 | 122.40 | 20.22 | 6.05 | 5.95 | 2.49 | 1.71 | 0.98 | 1.03 |
IIML88 | 2.67 | 0.39 | 29.98 | 139.62 | 120.04 | 19.58 | 6.13 | 6.75 | 2.61 | 1.93 | 0.95 | 0.99 |
IIML89 | 2.89 | 0.43 | 28.89 | 143.94 | 124.80 | 19.14 | 6.52 | 6.37 | 2.62 | 1.60 | 0.93 | 1.01 |
IIML90 | 2.91 | 0.41 | 31.12 | 146.75 | 126.16 | 20.59 | 6.13 | 6.44 | 2.49 | 1.88 | 0.88 | 1.01 |
样品编号 | Rb | Ba | Th | U | K | Ta | Nb | Sr | P | Zr | Hf | Ti |
IIML42 | 288.25 | 341.70 | 9.35 | 2.23 | 25 741.60 | 0.80 | 11.35 | 209.49 | 1 310.70 | 219.10 | 5.61 | 5 376.90 |
IIML84 | 210.93 | 310.53 | 7.09 | 2.04 | 25 588.81 | 0.84 | 10.99 | 478.30 | 1 294.78 | 282.57 | 6.39 | 6 261.00 |
IIML88 | 144.13 | 281.42 | 6.57 | 2.24 | 20 711.10 | 0.74 | 10.36 | 388.47 | 1 387.63 | 270.59 | 6.39 | 6 338.61 |
IIML89 | 92.83 | 292.51 | 7.46 | 1.97 | 16 541.58 | 0.78 | 10.9 | 459.31 | 1 253.86 | 285.18 | 6.70 | 5 971.83 |
IIML90 | 139.32 | 373.38 | 7.10 | 1.92 | 21 083.14 | 0.82 | 11.37 | 487.04 | 1 160.84 | 296.11 | 6.61 | 6 199.62 |
Fig.6 Chondrite-normalized REE patterns (a) and primitive mantle-normalized multi-element spider diagram (b) of the diorite porphyrite in Shazhangtu mining area(chondrite normalizing values after reference [25] and primitive mantle-normalizing values after reference [26])
测点号 | T/Ma | 176Yb/177Hf | 176Lu/177Hf | 176Hf/177Hf ±2σ | 176Hf/177Hf | εHf(0) | εHf(t) | TDM/Ma | | fLu/Hf |
---|---|---|---|---|---|---|---|---|---|---|
IIML84-1 | 309.1 | 0.046 1 | 0.001 2 | 0.282 720±0.000 024 | 0.282 713 | -1.8 | 4.7 | 758 | 1 024 | -0.96 |
IIML84-2 | 312.1 | 0.039 7 | 0.001 0 | 0.282 677±0.000 021 | 0.282 672 | -3.3 | 3.3 | 814 | 1 115 | -0.97 |
IIML84-5 | 316.5 | 0.026 6 | 0.000 8 | 0.282 705±0.000 025 | 0.282 701 | -2.4 | 4.4 | 771 | 1 047 | -0.98 |
IIML84-6 | 309.7 | 0.073 3 | 0.002 0 | 0.282 660±0.000 025 | 0.282 649 | -3.9 | 2.5 | 861 | 1 168 | -0.94 |
IIML84-7 | 316.7 | 0.075 8 | 0.002 0 | 0.282 731±0.000 031 | 0.282 719 | -1.5 | 5.1 | 758 | 1 005 | -0.94 |
IIML84-8 | 310.7 | 0.050 4 | 0.001 4 | 0.282 807±0.000 025 | 0.282 799 | 1.2 | 7.8 | 637 | 827 | -0.96 |
IIML84-11 | 314.4 | 0.036 6 | 0.000 9 | 0.282 686±0.000 022 | 0.282 681 | -3.0 | 3.7 | 801 | 1 093 | -0.97 |
IIML84-12 | 310.0 | 0.080 6 | 0.002 0 | 0.282 771±0.000 028 | 0.282 759 | 0.0 | 6.4 | 701 | 9 8 | -0.94 |
IIML84-15 | 314.6 | 0.034 8 | 0.001 0 | 0.282 613±0.000 022 | 0.282 607 | -5.6 | 1.1 | 905 | 1 259 | -0.97 |
IIML84-16 | 311.0 | 0.052 1 | 0.001 3 | 0.282 703±0.000 027 | 0.282 696 | -2.4 | 4.1 | 784 | 1 061 | -0.96 |
IIML84-19 | 313.8 | 0.056 6 | 0.001 4 | 0.282 785±0.000 028 | 0.282 777 | 0.5 | 7.1 | 669 | 876 | -0.96 |
Table 4 LA-ICP-MS zircon Hf isotope data of the diorite porphyrite in Shazhangtu mining area
测点号 | T/Ma | 176Yb/177Hf | 176Lu/177Hf | 176Hf/177Hf ±2σ | 176Hf/177Hf | εHf(0) | εHf(t) | TDM/Ma | | fLu/Hf |
---|---|---|---|---|---|---|---|---|---|---|
IIML84-1 | 309.1 | 0.046 1 | 0.001 2 | 0.282 720±0.000 024 | 0.282 713 | -1.8 | 4.7 | 758 | 1 024 | -0.96 |
IIML84-2 | 312.1 | 0.039 7 | 0.001 0 | 0.282 677±0.000 021 | 0.282 672 | -3.3 | 3.3 | 814 | 1 115 | -0.97 |
IIML84-5 | 316.5 | 0.026 6 | 0.000 8 | 0.282 705±0.000 025 | 0.282 701 | -2.4 | 4.4 | 771 | 1 047 | -0.98 |
IIML84-6 | 309.7 | 0.073 3 | 0.002 0 | 0.282 660±0.000 025 | 0.282 649 | -3.9 | 2.5 | 861 | 1 168 | -0.94 |
IIML84-7 | 316.7 | 0.075 8 | 0.002 0 | 0.282 731±0.000 031 | 0.282 719 | -1.5 | 5.1 | 758 | 1 005 | -0.94 |
IIML84-8 | 310.7 | 0.050 4 | 0.001 4 | 0.282 807±0.000 025 | 0.282 799 | 1.2 | 7.8 | 637 | 827 | -0.96 |
IIML84-11 | 314.4 | 0.036 6 | 0.000 9 | 0.282 686±0.000 022 | 0.282 681 | -3.0 | 3.7 | 801 | 1 093 | -0.97 |
IIML84-12 | 310.0 | 0.080 6 | 0.002 0 | 0.282 771±0.000 028 | 0.282 759 | 0.0 | 6.4 | 701 | 9 8 | -0.94 |
IIML84-15 | 314.6 | 0.034 8 | 0.001 0 | 0.282 613±0.000 022 | 0.282 607 | -5.6 | 1.1 | 905 | 1 259 | -0.97 |
IIML84-16 | 311.0 | 0.052 1 | 0.001 3 | 0.282 703±0.000 027 | 0.282 696 | -2.4 | 4.1 | 784 | 1 061 | -0.96 |
IIML84-19 | 313.8 | 0.056 6 | 0.001 4 | 0.282 785±0.000 028 | 0.282 777 | 0.5 | 7.1 | 669 | 876 | -0.96 |
Fig.8 Y-Sr/Y diagram ((a),base map according to reference [42]) and Ba/La-Th/Yb diagram ((b),base map according to reference [43]) of the diorite porphyry in Shazhangtu mining area
[1] | 李利阳, 刘博, 陈满, 等. 内蒙古阿巴嘎旗宝力高庙组一段沉积地质特征与构造属性[J]. 现代矿业, 2017(3):116-118,122. |
[2] | 鲁庆伟, 田麒, 王根厚, 等. 内蒙古阿巴嘎旗宝力高庙组地层划分及年代探讨[J]. 西部资源, 2016, 17(4):67-69. |
[3] | 宝音乌力吉, 赵文涛, 包凤琴. 内蒙古二连浩特—阿巴嘎旗北部宝力高庙组火山岩特征及构造背景[J]. 地质与资源, 2013, 22(5):355-359. |
[4] | 弓贵斌, 王全旗. 内蒙古自治区阿巴嘎旗地区上石炭统至下二叠统宝力高庙组火山岩特征与环境研究[J]. 西部资源, 2011, 12(2):69-73. |
[5] | 刘博. 内蒙古阿巴嘎旗地区宝力高庙组火山岩特征及成因研究[D]. 长春: 吉林大学, 2017. |
[6] | 贺淑赛, 李秋根, 王宗起, 等. 内蒙古中部宝力高庙组长英质火山岩 U-Pb-Hf 同位素特征及其地质意义[J]. 北京大学学报(自然科学版), 2015, 51(1):50-64. |
[7] | 王继春, 王银宏, 张梅, 等. 内蒙古高尔旗银铅锌矿区花岗岩的岩石成因: 地球化学、锆石U-Pb年代学及Hf同位素约束[J]. 现代地质, 2016, 30(5): 961-980. |
[8] | 贡二辰, 晁代超, 张喜周, 等. 内蒙古哈达特陶勒盖铅锌很多金属矿成矿地质特征及其成因[J]. 现代地质, 2013, 27(2):324-331. |
[9] | 张玉清, 张建, 屈强, 等. 内蒙古阿德拉嘎乌拉正长花岗岩锆石U-Pb年龄[J]. 地质与资源, 2013, 22(4):308-312. |
[10] | 邵积东, 王惠, 张梅, 等. 内蒙古大地构造单元划分及其地质特征[J]. 西部资源, 2011, 12(1):51-56. |
[11] | 郭灵俊, 赵志军, 崔来旺, 等. 内蒙古阿巴嘎旗北部铜多金属矿地质矿产特征及找矿方向[J]. 地球学报, 2011, 32(1):57-63. |
[12] |
ZONG K Q, KLEMD R, YUAN Y, et al. The assembly of Rodinia: The correlation of early Neoproterozoic (ca. 900 Ma) high-grade metamorphism and continental arc formation in the southern Beishan Orogen, southern Central Asian Orogenic Belt (CAOB)[J]. Precambrian Research, 2017, 290:32-48.
DOI URL |
[13] |
LIU Y S, HU Z C, GAO S, et al. In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard[J]. Chemical Geology, 2008, 257:34-43.
DOI URL |
[14] |
LIU Y S, GAO S, HU Z C, et al. Continental and oceanic crust recycling-induced melt-peridotite interactions in the Trans-North China Orogen: U-Pb dating, Hf isotopes and trace elements in zircons of mantle xenoliths[J]. Journal of Petrology, 2010, 51: 537-571.
DOI URL |
[15] |
ANDERSONT T. Correction of common lead in the U-Pb analyses that do not report 204Pb[J]. Chemical Geology, 2012, 192(1/2): 59-79.
DOI URL |
[16] | LUDWIG K R. Isoplot 3.00: A Geochronological Toolkit for Microsoft Excel[M]. Berkeley: Berkeley Geochronology Center, 2003. |
[17] | 耿建珍, 李怀坤, 张健, 等. 锆石Hf同位素组成的LA-MC-ICP-MS测定[J]. 地质通报, 2011, 30(10):34-39. |
[18] | 吴元保, 郑永飞. 锆石成因矿物学研究及其对U-Pb年龄解释的制约[J]. 科学通报, 2004, 49(16):1589. |
[19] | HANCHAR J M. Zircon zonation patterns as revealed by catho-doluminescence and backscattered electron images: implications for interpretation of complex crustal histories[J]. ChemicalGeology, 1993: 110. |
[20] |
BELOUSOVA E, GRIFFIN W, O’REILLY S Y, et al. Igneous zircon: trace element composition as an indicator of source rock type[J]. Contributions to Mineralogy and Petrology, 2002, 143(5):602-622.
DOI URL |
[21] |
MIDDLEMOST E. Naming materials in the magma/igneous rock system[J]. Earth-Science Reviews, 1994, 37(3/4):215-224.
DOI URL |
[22] | MIDDLEMOST E. A simple classification of volcanic rocks[J]. Bulletin of Volcanology, 1972, 36(2): 382-397. |
[23] | EWART A. The mineralogy and petrology of Tertiary-recent orogenic volcanic rocks: with special reference to the andesitic-basaltic compositional range[J]. Andesite, 1983(1): 25-87. |
[24] |
PICCOLI P. Tectonic discrimination of granitoids[J]. GSA Bulletin, 1989, 101(5): 635-643.
DOI URL |
[25] |
SUN S S, MCDONOUGH W F. Chemical and isotopic systematics of oceanic basalts: Implications for mantle composition and processes[J]. Geological Society,London,Special Publications, 1989, 42(1):313-345.
DOI URL |
[26] | BOYNTON W V. Cosmochemistry of the rare earth elements: meteorite studies[M]//Developments in Geochemistry. Amstordam:Elsevier, 1984: 63-114. |
[27] | 吴福元, 李献华, 郑永飞, 等. Lu-Hf 同位素体系及其岩石学应用[J]. 岩石学报, 2007, 23(2): 185-220. |
[28] | AMELIN Y, LEE D C, HALLIDAY A N, et al. Nature of the Earth’s earliest crust from hafnium isotopes in single detrital zircons[J]. Nature, 1999, 399:1497-1503. |
[29] |
VERVOORT J D, BLICHERT-TOFT J. Evolution of the depleted mantle: Hf isotope evidence from juvenile rocks through time[J]. Geochimica et Cosmochimica Acta, 1999, 63(3/4):533-556.
DOI URL |
[30] |
GRIFFIN W L, WANG X, JACKSON S E, et al. Zircon che-mistry and magma mixing,SE China: In-situ analysis of Hf isotopes, Tonglu and Pingtan igneous complexes[J]. Lithos, 2002, 61(3/4): 237-269.
DOI URL |
[31] |
RATAJESKI K, SISSON T W, GLAZNER A F, et al. Experimental and geochemical evidence for derivation of the El Capitan granite,California,by partial melting of hydrous gabbroic lower crust[J]. Contributions to Mineralogy and Petrology, 2005, 149(6):713-734.
DOI URL |
[32] |
VERVOORT J D, PATCHETT P J, GEHRELS G E, et al. Constraints on early Earth differentiation from hafnium and neodymium isotopes[J]. Nature, 1996, 379:624-627.
DOI URL |
[33] | 聂凤军. 中蒙边境中东段金属矿床成矿规律和找矿方向[M]. 北京: 地质出版社, 2007. |
[34] | 王继春. 内蒙古二连—东乌旗成矿带西段区域成矿系统研究及找矿预测[D]. 北京: 中国地质大学(北京), 2017. |
[35] | 陶继雄, 钟仁, 赵月明, 等. 内蒙古苏尼特左旗乌兰德勒钼(铜)矿床地质特征及找矿标志[J]. 地球学报, 2010, 31(3):413-422. |
[36] | 李蒙文. 天山—兴蒙造山带中段内生金属矿床成矿系列及成矿预测[D]. 北京: 中国地质科学院, 2006. |
[37] | 童英, 洪大卫, 王涛, 等. 中蒙边境中段花岗岩时空分布特征及构造和找矿意义[J]. 地球学报, 2010, 31(3): 395-412. |
[38] | 李可, 张志诚, 冯志硕, 等. 兴蒙造山带中段北部晚古生代两期岩浆活动及其构造意义[J]. 地质学报, 2015, 89(2):272-288. |
[39] | 云飞, 聂凤军, 江思宏, 等. 内蒙古莫若格钦地区二长闪长岩锆石 SHRIMP U-Pb年龄及其地质意义[J]. 矿床地质, 2011, 30(3):504-510. |
[40] | 余超, 柳振江, 宓奎峰, 等. 内蒙古巴彦都兰铜矿地质特征及矿床成因——岩石地球化学、 锆石 U-Pb 年代学及Hf同位素证据[J]. 现代地质, 2017, 31(6): 1095-1113. |
[41] |
WOOD D A, JORON J L, TREUIL M, et al. Elemental and Sr isotope variations in basic lavas from Iceland and the surrounding ocean floor[J]. Contributions to Mineralogy and Petrology, 1979, 70(3): 319-339.
DOI URL |
[42] |
DEFANT M J, DRUMMOND M S. Derivation of some modern arc magmas by melting of young subducted lithosphere[J]. Nature, 1990, 347: 662-665.
DOI URL |
[43] |
WOODHEAD J D, HERGT J M, DAVIDSON J P, et al. Hafnium isotope evidence for ‘conservative’ element mobility during subduction zone processes[J]. Earth and Planetary Science Letters, 2001, 192(3): 331-346.
DOI URL |
[44] |
KELEMEN P B, SHIMIZU N, DUNN T. Relative depletion of niobium in some arc magmas and the continental crust: partitioning of K,Nb,La and Ce during melt/rock reaction in the upper mantle[J]. Earth and Planetary Science Letters, 1993, 120: 111-134.
DOI URL |
[45] | WU P F, SUN D Y, WANG T H, et al. Chronology,geochemical characteristic and petrogenesis analysis of diorite in Helong of Yanbian area,NE China[J]. Geological Journal of China Universities, 2013, 19(4): 600-610. |
[46] | 邱婵媛, 肖倩茹, 魏永峰, 等, 冈底斯带西北缘别若则错地区晚白垩世闪长岩LA-ICP-MS锆石U-Pb测年、地球化学及地质意义[J]. 地质学报, 2018, 92(11): 2215-2226. |
[47] |
GREEN T H. Significance of Nb/Ta as an indicator of geochemical processes in the crust-mantle system[J]. Chemical Geology, 1995, 120(3/4):347-359.
DOI URL |
[48] |
KEPEZHINSKAS P, MCDERMOTT F, DEFANT M J. Trace element and Sr-Nd-Pb isotopic constraints on a three-component model of Kamchatka arc petrogenesis[J]. Geochimica et Cosmochimica Acta, 1997, 61(3): 577-600.
DOI URL |
[49] |
SCHERER E. Calibration of the lutetium-hafnium clock[J]. Science, 2001, 293:683-687.
DOI URL |
[50] | 孙立新, 任邦方, 赵凤清, 等. 内蒙古锡林浩特地块中元古代花岗片麻岩的锆石U-Pb年龄和 Hf 同位素特征[J]. 地质通报, 2013, 32(2/3): 327-340. |
[51] |
DOBRETSOV N L, BERZIN N A, BUSLOV M M. Opening and tectonic evolution of the Paleo-Asian Ocean[J]. International Geology Review, 1995, 37(4):335-360.
DOI URL |
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